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1.
Two new brown algae from the Xisha Islands,South China Sea 总被引:1,自引:0,他引:1
C.K.Tseng 《中国海洋湖沼学报》1983,1(2):185-189
In our phycological trips to the Xisha Islands,Guangdong Province,South ChinaSea in 1976 and 1980,two interesting brown algae had attracted our special attention.Oneof them was a Hydroclathrus,evidently more delicate and slender than H.clathratus com-monly met with in the South China Sea region.The other was a Turbinaria,characterizedby especially small leaves.Comparative studies of the two algae with other known speciesof the two genera concerned showed sufficient differences to warrant their statuses as un- 相似文献
2.
The aeolianite deposits on Shidao Island of the Xisha Islands,the South China Sea,contain five stages of aeolian biocalcarenites and four paleosols.The aeolian biocalcarenites consist of two sedimentary facies:dune and interdune deposits.In the dunes,large-scale festoon cross-bedding,humped cross-bedding and high-angle foreset bedding are well developed,and in the interdunes,large-scale flat-bedding and low-angle wedge shaped cross-bedding are well developed.The sedimentary structures and lamella features indicate that the aeolian deposits are driven mainly by the northeast monsoon.The aeolian biocalcarenite and paleosols may reflect the arid and humid climates of the East Asian monsoon,respectively.By comparison with the stalagmite oxygen isotope climosequence of Hulu Cave,Nanjing,we inferred that the aeolianite formed in the last glacial stage,and the paleosols were formed during relatively long-term warm events. 相似文献
3.
邢福武,李泽贤,叶华谷,陈炳辉,吴德邻ASTUDYONTHEFLORISTICPLANTGEOGRAPHYOFXISHAISLANDS,SOUTHCHINA¥XingFuwu;LiZexian;YeHuagu;ChenBinghui;WuDelin(... 相似文献
4.
C.K.Tseng 《中国海洋湖沼学报》1983,1(2):190-197
The genus Geppellais a small group of tropical and subtropical algae.It was establishedby Boergesen in 1940 on the basis of its uncalciferous frond and its characteristic of annularattachments of the filaments,with G.mortensenii Boergesen as the type of the genus.Sincethen four more species have been described,namely,G.decussata Dawson(1959),G.echino-caulos Cribb(1960),G.yaeyamense Tanaka(1963),and G.japonica Tanaka et Itono(1977).The species G.decussata was reported by Dawson from Isla San Francisco(Gulf of California)and the Marshall Islands,central Pacific,and later removed by Tanaka and Itono(1977)from the genus Geppella because of the absence of blade and of annular attachments of 相似文献
5.
unomicrroNTherearereportedstudisoninorganicsulfurcomPoundsinrnarinesedtritS(Song,l99(),Stefan,l994),butfeWonorganicsulfurcomPounds.Itwasshownthatthroughoilspthe,mnoffandatmosphdriproasses,manyanthropogedcorganicsulfurcomP0undsrnaybethenspotalintothemarineenvirorstWheretheycanbeeventuallydePositalalongwithnatamlorganicstilfUrcomPoundsinseddritSraateSetal.,l979).ResearchesonorganicstilfurcomPoundsinrnarinesedirnentSareofpotentialenvirornnentalchdricalshoilicanceforhaherunderstandingofthege… 相似文献
6.
Volcanic detrital sediments are a unique indicator for reconstructing the petrogenetie evolution of submarine volcanic terrains. Volcanic ash in surficial sediments around the Zhongsha Islands includes three kinds of volcanogenic detritus, i.e., brown volcanic glass, colorless volcanic glass and volcanic scoria. The major element characteristics show that bimodal volcanic activity may have taken place in the northern margin of the South China Sea, with brown volcanic glass and colorless volcanic glass repre-senting the maric end-member and felsie end-member, respectively. Fractional crystallization is the main process for magma evolu-tion. The nature of the volcanic activity implies that the origin of volcanic activity was related to extensional tectonic settings, which is corresponding to an extensional geodynamie setting in the Xisha Trench, and supports the notion, which is based on geophysical data and petrology, that there may exist a mantle plume around the Hainan Island. 相似文献
7.
《中国海洋湖沼学报》2017,(3)
Coral reefs in the Xisha Islands(also known as the Paracel Islands in English), South China Sea, have experienced dramatic declines in coral cover. However, the current regional scale hard coral distribution of geomorphic and ecological zones, essential for reefs management in the context of global warming and ocean acidification, is not well documented. We analyzed data from field surveys, Landsat-8 and GF-1 images to map the distribution of hard coral within geomorphic zones and reef flat ecological zones. In situ surveys conducted in June 2014 on nine reefs provided a complete picture of reef status with regard to live coral diversity, evenness of coral cover and reef health(live versus dead cover) for the Xisha Islands. Mean coral cover was 12.5% in 2014 and damaged reefs seemed to show signs of recovery. Coral cover in sheltered habitats such as lagoon patch reefs and biotic dense zones of reef flats was higher, but there were large regional differences and low diversity. In contrast, the more exposed reef slopes had high coral diversity, along with high and more equal distributions of coral cover. Mean hard coral cover of other zones was 10%. The total Xisha reef system was estimated to cover 1 060 km~2, and the emergent reefs covered ~787 km~2. Hard corals of emergent reefs were considered to cover 97 km~2. The biotic dense zone of the reef flat was a very common zone on all simple atolls, especially the broader northern reef flats. The total cover of live and dead coral can reach above 70% in this zone, showing an equilibrium between live and dead coral as opposed to coral and algae. This information regarding the spatial distribution of hard coral can support and inform the management of Xisha reef ecosystems. 相似文献
8.
中新统海相烃源岩是中国近海莺歌海盆地主要油气供给层段,也是我国新生代海相烃源岩的典型代表。综合利用地质、地球化学和古生物等资料,在烃源岩有机地球化学特征分析的基础上,探讨了莺歌海盆地中新统海相烃源岩发育的主控因素,并建立了相应的形成模式。结果表明,莺歌海盆地发育中等-好级别的中新统海相烃源岩,并具有较强的横向与纵向非均质性;中新统海相烃源岩受古气候、古生产力、水介质条件、沉积速率及海平面变化等因素的综合影响,发育以莺东斜坡带梅山组、三亚组为代表的海相陆源型和以东方区、乐东区梅山组为代表的海相内源型2种模式,其中以海相内源型烃源岩生烃条件最为优越。 相似文献
9.
《中国海洋大学学报(英文版)》2019,(6)
Based on the concentrations of the trace elements, rare earth elements(REE), and Sr isotopic compositions in reef carbonates from the well ‘Xike-1' reef core of the Xisha Islands, the constraints on sediment provenance and paleoenvironment were defined. Variations of the terrigenous input into the paleoseawater were traced in detail and the paleoenvironment and sediment provenance were further investigated. The results show that the HREE/LREE values in the reef carbonates are negatively associated with their Th and Al concentrations; however, their Al and Th concentrations show positive correlation. The lowest 87 Sr/86 Sr values in the reef carbonates generally coincide with the lowest values of Al, Th concentrations and the highest values of HREE/LREE. These data indicate that the HREE/LREE, Al concentrations, and Th concentrations of the reef carbonates are useful indexes for evaluating the influence of the terrigenous inputs on the seawater composition in the study area. From top to bottom, the changing process of the HREE/LREE values and Al, Th concentrations can be divided into 6 intervals; they are H1(0–89.30 m, about 0–0.11 Myr), L1(89.30–198.30 m, about 0.11–2.2 Myr), H2(198.30–374.95 m, about 2.2–5.3 Myr), D(374.95–758.40 m, about 5.3–13.6 Myr), L2(758.40–976.86 m, about 13.6–15.5 Myr), and H3(976.86–1200.00 m, about 15.5–21.5 Myr). Moreover, the changing trend of the HREE/LREE values coincides with that of the seawater δ~(13)C values recorded by benthonic foraminiferal skeletons from the drill core of ODP site 1148 in the South China Sea(SCS), but not with that of the seawater δ~(18)O values. The high uplifting rates of the Qinghai-Tibet Plateau coincide with the high Th and Al concentrations and the low HREE/LREE values in the reef carbonates. These data indicate that the main factors controlling the changes of terrigenous flux in the SCS are the tectonic activities associated with Qinghai-Tibet Plateau uplifting and the variations of uplifting rates rather than paleoclimatic changes. 相似文献
10.
11.
Fourteen isolated drowned reefs have been identified around the Xisha Uplift by multibeam and seismic data. The drowning processes of these reefs can be divided into three different stages, which correspond to three different accelerated tectonic subsidence periods. The drowning of the Xisha reefs is the result of the combined action of tectonic subsidence and sea level fluctuations, and the tectonic subsidence rate had to remain above 0.2 mm yr~(-1 )for a long time. Three abrupt accelerated tectonic subsidence events that occurred in the late Miocene, Pliocene and early Quaternary in the Xisha Uplift were closely related to the thermal subsidence processes after three stages of post-rifting magmatism. The magmatism of the middle Miocene and the following thermal subsidence resulted in the drowning of reefs in the northwestern Xisha uplift(Zone A). During the early Pliocene, massive magmatic intrusions and volcanic eruptions occurred in the Xisha Uplift. Then, the subsequent thermal subsidence started the drowning process of reefs in the northeastern and western regions of the Xisha Uplift(Zone B and C). During the early Quaternary, large-scale magmatism also occurred in the Xisha Uplift. The subsequent thermal subsidence resulted in a new rapid tectonic subsidence, which caused the reefs in the southern and southeastern regions of the Xisha Uplift to drown(Zone D and E). 相似文献
12.
《中国海洋湖沼学报》2016,(4)
Accumulation of metals in both sediments and Phragmites australis organs was studied. Samples were collected from seven stations located in Anzali wetland, Iran. The samples were analyzed by inductively coupled plasma mass spectrometry(ICP-MS). The results showed that concentration of the studied metals(except As and Cd) were higher in sediments than in P.australis organs. Metal accumulation was found to be signifi cantly(P 0.05) higher in roots than in above-ground organs of P.australis. The bioaccumulation factor(BAF) and the transfer factor(TF) also verifi ed the highest rate of metal accumulation in roots and their reduced mobility from roots to the above-ground organs. Pearson correlation coeffi cient showed signifi cant relationships between metal concentrations in sediments and those in plant organs. It should be pointed out that sediment and plant samples exhibited higher metal concentrations in eastern and central parts than in western and southern parts of the wetland. The mean concentrations of all studied elements(except for Fe, V and Al) were higher in these sediment samples than in the Earth's crust and shale. High accumulation of metals in P. australis organs(roots and shoots) is indicative of their high bioavailability in sediments of the wetland. The correlation between metal concentrations in sediments and in P. australis indicates that plant organs are good bioindicators of metal pollution in sediments of Anzali wetland. 相似文献
13.
The Gulf of Suez Basin is a very mature and extremely prospective petroleum province.Many heavy oil fields have been found in the Basin, and such reserves are abundant.Characteristics and models of heavy oil are analyzed in this study based on tectonic, basin evolution, stratigraphic distribution and geochemical data. The best reservoirs of heavy oil are Miocene sandstone and limestone formations.Source rocks of hydrocarbon include deep limestone and shale of the Brown Limestone, the Thebes Formation and the Rudeis Formation. Thick evaporite rocks with rock salts and anhydrites deposited broadly throughout the basin are the most impor-tant regional seals, whereas Miocene shales are intraformational and regional seals that cover small areas.Heavy oil could be directly generated or densified during vertical migration along faults and reservoir accumulation. The heavy oil accumulation model is a mixed model that includes three mechanisms:fault dispersal, sulfocom-pound reactions and hydrocarbons generated from immature source rock.After analyzing the model and the dis-tribution of source rocks, reservoirs, heavy oil fields and structures, it is concluded that the potential heavy oil area is at the center of the basin. 相似文献
14.
DONG Linsen SHI Xuefa LIU Yanguang FANG Xisheng CHEN Zhihua WANG Chunjuan ZOU Jianjun HUANG Yuanhui 《极地研究(英文版)》2014,(3):192-203
Mineralogical analysis was performed on bulk sediments of 79 surface samples using X-ray diffraction. The analytical results, combined with data on ocean currents and the regional geological background, were used to investigate the mineral sources. Mineral assemblages in sediments and their distribution in the study area indicate that the material sources are complex. (1) Feldspar is abundant in the sediments of the middle Chukchi Sea near the Bering Strait, originating from sediments in the Anadyr River carried by the Anadyr Current. Sediments deposited on the western side of the Chukchi Sea are rich in feldspar. Compared with other areas, sediments in this region are rich in hornblende transported from volcanic and sedimentary rocks in Siberia by the Anadyr Stream and the Siberian Coastal Current. Sediments in the eastern Chukchi Sea are rich in quartz sourced from sediments of the Yukon and Kuskokwim rivers carried by the Alaska Coastal Current. Sediments in the northern Chukchi Sea are rich in quartz and carbonates from the Mackenzie River sediments. (2) Sediments of the southern and central Canada Basin contain little calcite and dolomite, mainly due to the small impact of the Beaufort Gyre carrying carbonates from the Canadian Arctic Islands. Compared with other areas, the mica content in the region is high, implying that the Laptev Sea is the main sediment source for the southern and central Canada Basin. In the other deep sea areas, calcite and dolomite levels are high caused by the input of large amounts of sediment carried by the Beaufort Gyre from the Canadian Arctic Islands (Banks and Victoria). The Siberian Laptev Sea also provides small amounts of sediment for this region. Furthermore, the Atlantic mid-water contributes some fine-grained material to the entire deep western Arctic Ocean. 相似文献
15.
Examination of solvent-extractable lipids in sediments from Beibu Gulf, South China Sea by capillary gas chromatography (GC)
and capillary gas chromatography-mass spectrometry (GC-MS) resulted in the first identifications of β, γ-carotanes and their
C19 to C31 homologs in the modern sediments from the China Seas. Distributional features of these (mainly triterpenoid and steroid hydrocarbons)
biomarkers are discussed and the possibility of using these compounds as indicators of source of materials, diagenesis and
depositional conditions is explored. It was found that the biomarkers in this region are mixtures of allochthonous (terrigenous
and/or crude oil leak or pollution) and antochthonous (marine) organic components. The biomarders have proved to be of value
for understanding sedimentation.
Contribution No. 1888 from the Institute of Oceanology, Academia Sinica.
This research is partially funded by the Organic Geochemistry Laboratory, Institute of Geochemistry. Academia Sinica. 相似文献
16.
《东北石油大学学报》2016,(2)
寒武系白云岩是塔东地区下古生界碳酸盐岩储层的重要岩石类型之一。为认识塔东地区寒武系白云岩的地球化学特征和成因机理,通过岩心及薄片观察,将研究区寒武系白云岩划分为微—细晶它形白云石、细—中晶自形白云石、中—粗晶白云石和鞍形白云石4种类型;结合阴极发光分析、微量元素测试、稀土元素分析、碳氧稳定同位素分析、流体包裹体测温和X线衍射有序度分析等,探讨研究区寒武系白云岩成因和白云化作用模式。结果表明:微—细晶它形白云石成因机制为准同生期高盐度白云化作用;细—中晶自形白云石成因机制为埋藏白云化作用;中—粗晶白云石成因机制可分为2种类型,即Ⅰ型为基性岩浆热液流体重结晶白云化作用,Ⅱ型为中酸性岩浆热液流体重结晶白云化作用;鞍形白云石成因机制也可分为2种类型,即Ⅰ型为基性岩浆热液白云化作用,Ⅱ型为中酸性岩浆热液白云化作用。该结果为研究区寒武系白云岩储层预测和油气勘探部署提供依据。 相似文献
17.
The underground water qualitymodel with non-linear inversion problem is illposed, and boils down to solving the minimum of nonlinear function. Genetic algorithms are adopted in a number of individuals of groups by iterative search to find the optimal solution of the problem, the encoding strings as its operational objective, and achieving the iterative calculations by the genetic operators. It is an effective method of inverse problems of groundwater, with incomparable advantages and practical significances. 相似文献
18.
MA Ruijie LI Xin. College of Mathematics Jilin University Changchun China . College of Construction Engineering China 《东北亚地学研究》2009,(3):164-167
The underground water quality model with non-linear inversion problem is ill-posed, and boils down to solving the minimum of nonlinear function. Genetic algorithms are adopted in a number of individuals of groups by iterative search to find the optimal solution of the problem, the encoding strings as its operational objective, and achieving the iterative calculations by the genetic operators. It is an effective method of inverse problems of groundwater, with incomparable advantages and practical significances. 相似文献
19.
我国海岛资源开发利用在环境、管理和经济等方面存在诸多问题。环境问题主要包括:海岛及其周围海域生物多样性的丧失,海岛淡水资源紧张,周围海域环境污染,陆海通道和围海工程造成海域自然环境状况改变;管理问题主要包括:海岛管理体制不健全,海岛资源权属不清,海岛开发管理法规不完善;经济问题主要包括:海岛地区经济基础薄弱,海岛开发产业布局不合理。最后提出我国海岛资源开发利用应该:建立有效的海岛综合管理体系和机构;因地制宜开发利用海岛资源;增加海岛资金投入,逐步扩大海岛对外开放力度;大力发展海岛科教事业, 实施人才战略。 相似文献
20.
The global climate is intimately connected to changes in the polar oceans. The variability of sea ice coverage affects deep-water formations and large-scale thermohaline circulation patterns. The polar radiative budget is sensitive to sea-ice loss and consequent surface albedo changes. Aerosols and polar cloud microphysics are crucial players in the radioactive energy balance of the Arctic Ocean. The main biogenic source of sulfate aerosols to the atmosphere above remote seas is dimethylsulfide (DMS). Recent research suggests the flux of DMS to the Arctic atmosphere may change markedly under global warming. This paper describes climate data and DMS production (based on the five years from 1998 to 2002) in the region of the Barents Sea (30–35°E and 70–80°N). A DMS model is introduced together with an updated calibration method. A genetic algorithm is used to calibrate the chlorophyll-a (CHL) measurements (based on satellite SeaWiFS data) and DMS content (determined from cruise data collected in the Arctic). Significant interannual variation of the CHL amount leads to significant interannual variability in the observed and modeled production of DMS in the study region. Strong DMS production in 1998 could have been caused by a large amount of ice algae being released in the southern region. Forcings from a general circulation model (CSIRO Mk3) were applied to the calibrated DMS model to predict the zonal mean sea-to-air flux of DMS for contemporary and enhanced greenhouse conditions at 70–80°N. It was found that significantly decreasing ice coverage, increasing sea surface temperature and decreasing mixed-layer depth could lead to annual DMS flux increases of more than 100% by the time of equivalent CO2 tripling (the year 2080). This significant perturbation in the aerosol climate could have a large impact on the regional Arctic heat budget and consequences for global warming. 相似文献